Getting Started
We will investigate what happens when a wave, such as a light ray or a ripple in a pond, reaches the end of its medium or encounters a different one. This chapter focuses on the interaction at the boundary between two distinct media. The core question is: How does a wave's energy and its fundamental properties—like speed, wavelength, and direction—change when it meets a new substance?
What You Should Be Able to Do
After completing this section, you will be able to:
Describe the two possible behaviors, reflection and transmission, that occur when a wave encounters a boundary.
Explain why a wave's frequency remains constant as it moves from one medium to another.
Predict how a wave's speed and wavelength change when it is transmitted across a boundary.
Define polarization and explain why it is a property exclusive to transverse waves.
Differentiate between transverse and longitudinal waves based on their capacity for polarization.
Key Concepts & Mechanisms
System & Preconditions
Our system consists of a wave, the initial medium it travels in, a second medium, and the boundary between them. We make several idealizations:
The media are uniform and isotropic, meaning their properties are the same everywhere and in all directions.
The boundary is a sharp, well-defined interface.
No energy is dissipated as thermal energy (absorption) at the boundary; all incident energy is either reflected or transmitted.
Key Steps / Relations
Incident Wave Approaches: A wave with a specific frequency, f (in Hertz, Hz), wavelength, (in meters, m), and wave speed, (in m/s), propagates through Medium 1. These properties are related by the universal wave equation: . The wave carries energy, proportional to the square of its amplitude.
Interaction at the Boundary: The incident wave reaches the boundary and exerts a periodic force on the particles of Medium 2. This interaction forces the boundary particles to oscillate. Crucially, the boundary particles are driven to oscillate at the exact same frequency, f, as the incoming wave.
Energy Partitioning: The oscillating particles at the boundary act as a new source, generating two separate waves:
A reflected wave that travels back into the original medium (Medium 1).
A transmitted wave that passes into the new medium (Medium 2).
The energy of the incident wave is split between the reflected and transmitted waves. By the principle of conservation of energy, the sum of the energy in the reflected and transmitted waves must equal the energy of the incident wave (assuming no absorption).
Frequency Conservation: Because the boundary oscillations that create the new waves are driven by the incident wave, their frequency is identical. Therefore, the frequency of the wave is the one quantity that remains constant throughout the entire interaction.
Changes in Wave Properties:
The wave speed is determined by the properties of the medium (e.g., tension and linear density for a string, or refractive index for light). Since the transmitted wave is in a new medium (Medium 2), its speed will change to . The reflected wave, remaining in Medium 1, retains the original speed, .
Since frequency (f) is constant but speed (v) changes for the transmitted wave, its wavelength must also change to satisfy the universal wave equation: .
Outputs & Effects
The primary effect of the interaction is the partitioning of the wave. An incoming wave is split into two outgoing waves.
Constant Quantity: Frequency (f).
Changed Quantities: For the transmitted wave, both wave speed (v) and wavelength () change. The amplitudes of both the reflected and transmitted waves are smaller than the incident wave's amplitude, as the initial energy is divided between them.
Regulation & Limits
This model holds for linear waves where the principle of superposition applies. The specific characteristics of reflection (such as whether a wave on a string reflects upright or inverted) depend on the relative properties of the two media (e.g., whether the second string is more or less dense). For light, these properties are captured by the index of refraction.
Polarization of Transverse Waves
A separate but related concept is polarization, which describes the orientation of a wave's oscillations.
| Feature | Transverse Waves (e.g., Light) | Longitudinal Waves (e.g., Sound) | Why It Matters |
|---|---|---|---|
| Oscillation Direction | Particle oscillation is perpendicular to the direction of energy propagation. | Particle oscillation is parallel to the direction of energy propagation. | This geometric difference is the fundamental reason why only transverse waves can be polarized. |
| Polarization | Can be polarized. The oscillations can be restricted to a single plane. For example, a vertical polarizing filter will only allow the vertical component of the wave's oscillation to pass through. | Cannot be polarized. Since the oscillation is already confined to one dimension (along the direction of travel), there is no other plane of oscillation to restrict. | Polarization is definitive experimental evidence that a wave is transverse. The fact that light can be polarized is key evidence that it is a transverse wave. |
| Example | Unpolarized light from the sun has electric field oscillations in all perpendicular planes. A polarizing filter blocks all but one of these planes. | Sound waves are compressions and rarefactions of the medium in the same direction the sound is traveling. There is no "side-to-side" motion to filter. | This distinction is used in many technologies, such as polarized sunglasses (to reduce glare, which is horizontally polarized light) and LCD screens. |
Key Models & Diagrams
This matrix connects the physical process at a boundary to its mathematical description and observable outcomes.
| Representation | Key Relations | Predicted Observables |
|---|
| Reflection & Transmission